Foraminifera taxon details

Matanzia Palmer, 1936 †

734642  (urn:lsid:marinespecies.org:taxname:734642)

accepted
Genus
Matanzia bermudezi Palmer, 1936 † (type by original designation)

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  1. Species Matanzia bermudezi Palmer, 1936 †
  2. Species Matanzia cibaoensis Bermúdez, 1949 †
  3. Species Matanzia incrassata Bermúdez, 1949 †
  4. Species Matanzia mahoenuia Finlay, 1939 †
  5. Species Matanzia margaritensis Bermúdez & Gámez, 1966 †
  6. Species Matanzia proxima Bermúdez, 1949 †
  7. Species Matanzia simulans Finlay, 1939 † accepted as Remesella varians (Glaessner, 1937) † (Subjective junior synonym in opinion of Kaminski and Gradstein (http://nhm2.uio.no/norges/atlas/index.htm))
  8. Species Matanzia varians (Glaessner, 1937) † accepted as Remesella varians (Glaessner, 1937) † (Opinion of Kaminski and Gradstein (http://nhm2.uio.no/norges/atlas/index.htm))
marine, brackish, fresh, terrestrial
fossil only
feminine
Palmer, D. K. (1936). New genera and species of Cuban Oligocene foraminifera. <em>Memorias de la Sociedad Cubana de Historia Natural Felipe Poey.</em> 10 (2): 123-128.
page(s): p. 125 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Matanzia Palmer, 1936 †. Accessed at: http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=734642 on 2024-02-29
Date
action
by
2013-07-15 12:00:40Z
created
2013-07-17 07:13:52Z
changed
2013-09-05 09:33:42Z
changed
2017-11-22 12:39:06Z
changed
2020-03-09 20:53:26Z
changed

original description Palmer, D. K. (1936). New genera and species of Cuban Oligocene foraminifera. <em>Memorias de la Sociedad Cubana de Historia Natural Felipe Poey.</em> 10 (2): 123-128.
page(s): p. 125 [details]  Available for editors  PDF available [request] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
From editor or global species database
Diagnosis Test elongate, cylindrical, up to 1.8 mm in length, trochospirally enrolled in the early stage, with up to five chambers per whorl, then rapidly reduced to biserial, the biserial stage occupying about half the test length, interior of chambers subdivided by up to ten narrow vertical partitions that radiate inward from the outer wall; wall agglutinated; aperture a low arch at the base of the final chamber. L. Oligocene to Miocene; Cuba; ?New Zealand. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]